User:DGShanks/Shetland Plate Draft
**All final edits are located in Main-space**
[edit]This page is used as a working/drafting space only and should not be considered final. All final edits will be copied into main-space.
Shetland Plate
[edit]The Shetland Plate is a tectonic microplate located off the tip of the Antarctic Peninsula and contains the South Shetland Islands.[1] The plate is bordered on three sides by the Antarctic Plate and the fourth side is bordered by the Scotia Plate. The northwestern border is defined by the South Shetland Trench separating the Shetland Plate to the south from the Antarctic Plate to the north. This trench is the remnant of a subduction zone where the defunct Phoenix Plate, now part of the Antarctic Plate, subducted under the Antarctic Peninsula and the Shetland Islands. The southeastern border is a rift zone with the Antarctic Plate creating the Bransfield Basin.[2] The southwestern and northeastern boundaries are each part of larger fracture zones. The southwestern border is the Hero Fracture Zone and separates the Antarctic Plate to the southwest from the Shetland Plate to the northeast. The northeastern boundary is the Shackleton Fracture Zone and separates the Shetland Plate to the southwest from the Scotia Plate.[1]
Geologic History
[edit]The Shetland Plate started forming 3 to 4 million years ago.[2] Prior to formation, the Shetland Plate was part of the Antarctic Plate adjacent to the Antarctic Peninsula. During this period the Phoenix Plate, to the northwest, was subducting under the Antarctic Peninsula and the South Shetland Islands, which created the South Shetland Trench.[3] Approximately 3 million years ago spreading stopped at the Antarctic-Phoenix spreading center in Drake Passage. The Phoenix Plate is now considered part of the larger Antarctic Plate due to a lack of relative movement between the two since spreading ceased.[3] However, subduction in the South Shetland Trench did not cease. Slab rollback of the former Phoenix Plate underneath the South Shetland Islands caused rifting to develop in the Antarctic Peninsula creating the Shetland Plate and the Bransfield Basin. Rifting centers in the Bransfield Basin continue to separate the Shetland Plate from the Antarctic Peninsula.[4]
Tectonic Setting
[edit]South Shetland Trench
[edit]The South Shetland Trench forms the northwest border of the Shetland Plate. The trench is formed by the subduction of the Antarctic Plate in the north under the Shetland Plate in the south.[2] Subduction along this trench has slowed significantly over time, from 4-6 cm/yr over the last 30 million years to 1-2 cm/yr in the last 6 million years.[3][5] Current subduction is caused by the movement of the Shetland Plate northward, as well as, slab rollback of the former Phoenix Plate.[4]
Bransfield Basin
[edit]The Bransfield Basin forms the southeast border of the Shetland Plate. The basin separates the Shetland Plate on the north and the Antarctic Plate to the south. The basin is a back-arc rift basin.[2] The basin ranges from 1300 to over 2700 meters deep.[6]
Shackleton Fracture Zone
[edit]The Shackleton Fracture Zone is the northeast border of the Shetland Plate.[5] The fracture zone is a series of parallel transform faults separating the Scotia Plate from the Shetland Plate. This border with the Scotia plate is the only Shetland Plate boundary that is not with the Antarctic Plate.[2]
Hero Fracture Zone
[edit]The Hero Fracture Zone is the southwest boundary of the Shetland Plate. This feature separates the Shetland Plate from the Antarctic Plate. These parallel faults connect the Bransfield Basin in the south to the South Shetland Trench in the north.[5]
Volcanism
[edit]Absolute K-Ar ages indicate volcanism has been active from the Cenozoic to the present. Current volcanism can be seen at places like Deception Island and Penguin Island. Calc-alkaline plutons, a type of magma seen above subduction zones, date from the Cenozoic to the Miocene and is coincident with the active subduction of the Phoenix plate under Antartica. More recent Pliocene dated volcanism in the Bransfield basin has transitional chemistry between subduction zone calc-alkaline and mid ocean ridge tholeiitic magmas. The transitional chemistry can be explained by back-arc rifting in the Bransfield Basin.[7][8]
Earthquakes
[edit]Since the early 1980s earthquakes have been recorded in the Shetland Plate. The amount of data has been limited by remoteness, severe weather, and a lack of permeant seismic stations in the area.[8][9] Intermediate depth earthquakes (35-55km) under the South Shetland Islands indicates that subduction is still occurring at the Shetland Trench.[8]
Also See
[edit]Unused References [10]
References
[edit]- ^ a b Berrocoso, M.; Fernández-Ros, A.; Prates, G.; García, A.; Kraus, S. "Geodetic implications on block formation and geodynamic domains in the South Shetland Islands, Antarctic Peninsula". Tectonophysics. 666: 211–219. doi:10.1016/j.tecto.2015.10.023.
- ^ a b c d e Bird, Peter (2003-03). "An updated digital model of plate boundaries". Geochemistry, Geophysics, Geosystems. 4 (3). doi:10.1029/2001gc000252. ISSN 1525-2027.
{{cite journal}}: Check date values in:|date=(help) - ^ a b c Vérard, Christian; Flores, Kennet; Stampfli, Gérard. "Geodynamic reconstructions of the South America–Antarctica plate system". Journal of Geodynamics. 53: 43–60. doi:10.1016/j.jog.2011.07.007.
- ^ a b Solari, M. A.; Hervé, F.; Martinod, J.; Roux, J. P. Le; Ramírez, L. E.; Palacios, C. (2008/04). "Geotectonic evolution of the Bransfield Basin, Antarctic Peninsula: insights from analogue models". Antarctic Science. 20 (2): 185–196. doi:10.1017/s095410200800093x. ISSN 1365-2079.
{{cite journal}}: Check date values in:|date=(help) - ^ a b c Jin, Young Keun; Lee, Joohan; Hong, Jong Kuk; Nam, Sang Heon (2009-03-01). "Is subduction ongoing in the South Shetland Trench, Antarctic Peninsula?: new constraints from crustal structures of outer trench wall". Geosciences Journal. 13 (1): 59–67. doi:10.1007/s12303-009-0005-5. ISSN 1226-4806.
- ^ Gràcia, Eulàlia; Canals, Miquel; Farràn, Marcel Lí; Prieto, Maria José; Sorribas, Jordi; Team, Gebra (1996-06-01). "Morphostructure and evolution of the central and Eastern Bransfield Basins (NW Antarctic Peninsula)". Marine Geophysical Researches. 18 (2–4): 429–448. doi:10.1007/BF00286088. ISSN 0025-3235.
- ^ González-Ferrán, O. "Volcanic and tectonic evolution of the Northern Antarctic Peninsula—Late Cenozoic to recent". Tectonophysics. 114 (1–4): 389–409. doi:10.1016/0040-1951(85)90023-x.
- ^ a b c Pelayo, Aristeo M.; Wiens, Douglas A. (1989). "Seismotectonics and relative plate motions in the Scotia Sea region". Journal of Geophysical Research. 94 (B6): 7293. doi:10.1029/jb094ib06p07293. ISSN 0148-0227.
- ^ Ibáñez, J. M.; Morales, J.; Alguacil, G.; Almendros, J.; Oritz, R.; Pezzo, E. Del (1997-03-01). "Intermediate-focus earthquakes under South Shetland Islands (Antarctica'". Geophysical Research Letters. 24 (5): 531–534. doi:10.1029/97gl00314. ISSN 1944-8007.
- ^ Schreider, Al A.; Schreider, A. A.; Galindo-Zaldivar, J.; Maldonado, A.; Gamboa, L.; Martos, Y.; Lobo, F.; Evsenko, E. I. (2015-02-01). "Structure of the Bransfield strait crust". Oceanology. 55 (1): 112–123. doi:10.1134/s0001437014060101. ISSN 0001-4370.